Evaluation of PRISMA products over snow in the Alps and Antarctica

PRISMA is a hyperspectral satellite mission launched by the Italian Space Agency (ASI) in April 2019. The mission is designed to collect data at global scale for a variety of applications, including those related to the cryosphere. This study presents an evaluation of PRISMA Level 1 (L1) and Level 2...

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Main Authors: Mauro, Biagio Di, Cogliati, Sergio, Bohn, Niklas, Traversa, Giacomo, Garzonio, Roberto, Tagliabue, Giulia, Bramati, Gabriele, Cremonese, Edoardo, Julitta, Tommaso, Guanter, Luis, Kokhanovsky, Alexander, Giardino, Claudia, Panigada, Cinzia, Rossini, Micol, Colombo, Roberto
Format: Other/Unknown Material
Language:unknown
Published: Authorea, Inc. 2023
Subjects:
Boa
Online Access:http://dx.doi.org/10.22541/essoar.170365189.95440911/v1
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spelling crwinnower:10.22541/essoar.170365189.95440911/v1 2024-06-02T07:57:47+00:00 Evaluation of PRISMA products over snow in the Alps and Antarctica Mauro, Biagio Di Cogliati, Sergio Bohn, Niklas Traversa, Giacomo Garzonio, Roberto Tagliabue, Giulia Bramati, Gabriele Cremonese, Edoardo Julitta, Tommaso Guanter, Luis Kokhanovsky, Alexander Giardino, Claudia Panigada, Cinzia Rossini, Micol Colombo, Roberto 2023 http://dx.doi.org/10.22541/essoar.170365189.95440911/v1 unknown Authorea, Inc. posted-content 2023 crwinnower https://doi.org/10.22541/essoar.170365189.95440911/v1 2024-05-07T14:19:16Z PRISMA is a hyperspectral satellite mission launched by the Italian Space Agency (ASI) in April 2019. The mission is designed to collect data at global scale for a variety of applications, including those related to the cryosphere. This study presents an evaluation of PRISMA Level 1 (L1) and Level 2 (L2D) products for different snow conditions. To the aim, PRISMA data were collected at three sites: two in the Western European Alps (Torgnon and Plateau Rosa) and one in East Antarctica (Nansen Ice Shelf). PRISMA data were acquired contemporary to both field measurements and Sentinel-2 data. Simulated Top of the Atmosphere (TOA) radiance data were then compared to L1 PRISMA and Sentinel-2 TOA radiance. Bottom Of Atmosphere (BOA) reflectance from PRISMA L2D and Sentinel-2 L2A data were then evaluated by direct comparison with field data.Both TOA radiance and BOA reflectance PRISMA products were generally in good agreement with field data, showing a Mean Absolute Difference (MAD) lower than 5%. L1 PRISMA TOA radiance products resulted in higher MAD for the site of Torgnon, which features the highest topographic complexity within the investigated areas. In Plateau Rosa we obtained the best comparison between PRISMA L2D reflectance data and in situ measurements, with MAD values lower than 5 % for the 400-900nm range. The Nansen Ice Shelf instead resulted in MAD values <10% between PRISMA L2D and field data, while Sentinel-2 BOA reflectance showed higher values than other data sources. Other/Unknown Material Antarc* Antarctica East Antarctica Ice Shelf The Winnower Boa ENVELOPE(15.532,15.532,66.822,66.822) East Antarctica Prisma ENVELOPE(-58.767,-58.767,-69.200,-69.200)
institution Open Polar
collection The Winnower
op_collection_id crwinnower
language unknown
description PRISMA is a hyperspectral satellite mission launched by the Italian Space Agency (ASI) in April 2019. The mission is designed to collect data at global scale for a variety of applications, including those related to the cryosphere. This study presents an evaluation of PRISMA Level 1 (L1) and Level 2 (L2D) products for different snow conditions. To the aim, PRISMA data were collected at three sites: two in the Western European Alps (Torgnon and Plateau Rosa) and one in East Antarctica (Nansen Ice Shelf). PRISMA data were acquired contemporary to both field measurements and Sentinel-2 data. Simulated Top of the Atmosphere (TOA) radiance data were then compared to L1 PRISMA and Sentinel-2 TOA radiance. Bottom Of Atmosphere (BOA) reflectance from PRISMA L2D and Sentinel-2 L2A data were then evaluated by direct comparison with field data.Both TOA radiance and BOA reflectance PRISMA products were generally in good agreement with field data, showing a Mean Absolute Difference (MAD) lower than 5%. L1 PRISMA TOA radiance products resulted in higher MAD for the site of Torgnon, which features the highest topographic complexity within the investigated areas. In Plateau Rosa we obtained the best comparison between PRISMA L2D reflectance data and in situ measurements, with MAD values lower than 5 % for the 400-900nm range. The Nansen Ice Shelf instead resulted in MAD values <10% between PRISMA L2D and field data, while Sentinel-2 BOA reflectance showed higher values than other data sources.
format Other/Unknown Material
author Mauro, Biagio Di
Cogliati, Sergio
Bohn, Niklas
Traversa, Giacomo
Garzonio, Roberto
Tagliabue, Giulia
Bramati, Gabriele
Cremonese, Edoardo
Julitta, Tommaso
Guanter, Luis
Kokhanovsky, Alexander
Giardino, Claudia
Panigada, Cinzia
Rossini, Micol
Colombo, Roberto
spellingShingle Mauro, Biagio Di
Cogliati, Sergio
Bohn, Niklas
Traversa, Giacomo
Garzonio, Roberto
Tagliabue, Giulia
Bramati, Gabriele
Cremonese, Edoardo
Julitta, Tommaso
Guanter, Luis
Kokhanovsky, Alexander
Giardino, Claudia
Panigada, Cinzia
Rossini, Micol
Colombo, Roberto
Evaluation of PRISMA products over snow in the Alps and Antarctica
author_facet Mauro, Biagio Di
Cogliati, Sergio
Bohn, Niklas
Traversa, Giacomo
Garzonio, Roberto
Tagliabue, Giulia
Bramati, Gabriele
Cremonese, Edoardo
Julitta, Tommaso
Guanter, Luis
Kokhanovsky, Alexander
Giardino, Claudia
Panigada, Cinzia
Rossini, Micol
Colombo, Roberto
author_sort Mauro, Biagio Di
title Evaluation of PRISMA products over snow in the Alps and Antarctica
title_short Evaluation of PRISMA products over snow in the Alps and Antarctica
title_full Evaluation of PRISMA products over snow in the Alps and Antarctica
title_fullStr Evaluation of PRISMA products over snow in the Alps and Antarctica
title_full_unstemmed Evaluation of PRISMA products over snow in the Alps and Antarctica
title_sort evaluation of prisma products over snow in the alps and antarctica
publisher Authorea, Inc.
publishDate 2023
url http://dx.doi.org/10.22541/essoar.170365189.95440911/v1
long_lat ENVELOPE(15.532,15.532,66.822,66.822)
ENVELOPE(-58.767,-58.767,-69.200,-69.200)
geographic Boa
East Antarctica
Prisma
geographic_facet Boa
East Antarctica
Prisma
genre Antarc*
Antarctica
East Antarctica
Ice Shelf
genre_facet Antarc*
Antarctica
East Antarctica
Ice Shelf
op_doi https://doi.org/10.22541/essoar.170365189.95440911/v1
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